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  2. Geography of Barbados - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Barbados

    Barbados. /  13.167°N 59.550°W  / 13.167; -59.550. Barbados is a continental island in the North Atlantic Ocean and is located at 13°10' north of the equator, and 59°32' west of the Prime Meridian. As the easternmost isle of the Lesser Antilles in the West Indies, Barbados lies 160 kilometres (100 mi) east of the Windward Islands and ...

  3. Tidal range - Wikipedia

    en.wikipedia.org/wiki/Tidal_range

    Tidal range. Tidal range is the difference in height between high tide and low tide. Tides are the rise and fall of sea levels caused by gravitational forces exerted by the Moon and Sun, by Earth's rotation and by centrifugal force caused by Earth's progression around the Earth-Moon barycenter. Tidal range depends on time and location.

  4. Barbados - Wikipedia

    en.wikipedia.org/wiki/Barbados

    Barbados ( UK: / bɑːrˈbeɪdɒs / bar-BAY-doss; US: / bɑːrˈbeɪdoʊs / bar-BAY-dohss; locally / bɑːrˈbeɪdəs / bar-BAY-dəss) is an island country in the Lesser Antilles of the West Indies, in the Caribbean region of North America, and is the most easterly of the Caribbean islands.

  5. Tide - Wikipedia

    en.wikipedia.org/wiki/Tide

    The water stops rising, reaching a local maximum called high tide. Sea level falls over several hours, revealing the intertidal zone; ebb tide. Oscillating currents produced by tides are known as tidal streams or tidal currents. The moment that the tidal current ceases is called slack water or slack tide. The tide then reverses direction and is ...

  6. Earth tide - Wikipedia

    en.wikipedia.org/wiki/Earth_tide

    Earth tide (also known as solid-Earth tide, crustal tide, body tide, bodily tide or land tide) is the displacement of the solid earth 's surface caused by the gravity of the Moon and Sun. Its main component has meter-level amplitude at periods of about 12 hours and longer. The largest body tide constituents are semi- diurnal, but there are also ...

  7. Internal tide - Wikipedia

    en.wikipedia.org/wiki/Internal_tide

    These sea surface expressions of the internal tide at different wavelengths can be detected with the Topex/Poseidon or Jason-1 satellites (Fig. 2). Near 15 N, 175 W on the Line Islands Ridge, the mode-1 internal tides scatter off the topography, possibly creating turbulence and mixing, and producing smaller wavelength mode 2 internal tides.

  8. Port of Bridgetown - Wikipedia

    en.wikipedia.org/wiki/Port_of_Bridgetown

    www .barbadosport .com. The Port of Bridgetown (officially the Deep Water Harbour ), [4] ( UN/LOCODE: BB BGI, Port Callsign: 8PB) is a seaport in Bridgetown on the southwest coast of Barbados. [5] Situated at the North-Western end of Carlisle Bay, the harbour handles all of the country's international bulk ship -based trade and commerce. [6]

  9. Geology of Barbados - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Barbados

    Geology of Barbados. The geology of the island Barbados includes exposures of reef-related carbonate rocks spanning 85 percent of the island's surface. This coral rock formation is 70 meters thick and dates to the Pleistocene. Unlike neighboring islands in the Lesser Antilles volcanic arc, Barbados is unusual because it is not a volcanic island ...